华北克拉通北缘中段多伦地区早二叠世双峰式岩浆作用

李天瑜; 李世超; 李鹏川; 彭云彪; 那木吉拉; 雒德利; 赵庆英; 孙加鹏

doi:10.3799/dqkx.2021.210

Volume 48 Issue 8

Aug. 2023

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Article Navigation > Earth Science > 2023 > 48(8): 2888-2904

Li Tianyu, Li Shichao, Li Pengchuan, Peng Yunbiao, Na Mujila, Luo Deli, Zhao Qingying, Sun Jiapeng, 2023. Early Permian Bimodal Magmatism in the Duolun Area of the Central Section of the Northern Margin of the North China Craton. Earth Science, 48(8): 2888-2904. doi: 10.3799/dqkx.2021.210

Citation:

Li Tianyu, Li Shichao, Li Pengchuan, Peng Yunbiao, Na Mujila, Luo Deli, Zhao Qingying, Sun Jiapeng, 2023. Early Permian Bimodal Magmatism in the Duolun Area of the Central Section of the Northern Margin of the North China Craton. Earth Science, 48(8): 2888-2904. doi: 10.3799/dqkx.2021.210

Citation:

Li Tianyu, Li Shichao, Li Pengchuan, Peng Yunbiao, Na Mujila, Luo Deli, Zhao Qingying, Sun Jiapeng, 2023. Early Permian Bimodal Magmatism in the Duolun Area of the Central Section of the Northern Margin of the North China Craton. Earth Science, 48(8): 2888-2904. doi: 10.3799/dqkx.2021.210

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Early Permian Bimodal Magmatism in the Duolun Area of the Central Section of the Northern Margin of the North China Craton

doi: 10.3799/dqkx.2021.210

1.
College of Earth Sciences, Jilin University, Changchun 130061, China
2.
No. 208 Geological Party, CNNC, Baotou 014010, China
3.
Key Laboratory of Mineral Resources Evaluation in Northeast Asia, Ministry of Natural Resources, Changchun 130061, China
4.
Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China

Received Date: 2021-12-28
Publish Date: 2023-08-25

Abstract

Abstract

This paper presents petrological, Hf isotopes, geochronological and geochemical study on the early Permian Bimodal magmatites in Duolun area, Inner Mongolia, which is tectonically located in the northern margin of North China Craton, comprising quartz monzonite and basalt. U-Pb dating of zircons from the samples by LA-ICP-MS yield weighed mean ²⁰⁶Pb/²³⁸U ages of 283±1.6 Ma and 280±2.9 Ma respectively. They have similar Hf isotopes. Hf isotopes t_DM2 was oldgenerally (from 1 760 to 2 354 Ma, merely two youngs: 324 Ma and 824 Ma) and closed to these reported in ancient basement of North China Plate. The quartz monzonite and basalt exhibit SiO₂ geochemical discontinuity (50.64%~65.87%), showing typically bimodal features. They also significantly enrich K, Na, Al and deplete Ca, Mg. Besides, the quartz monzonite show significantly depletions in Ti and P compared with the basalt, showing complementary relations. This paper, combined with previous data, suggest that Bimodal magmatitesare the products of partial melting of the ancient basement of the North China Plate under the background of extension, which was caused by the upward migrating and gathering of the mantle magma formed from partial melting of mantle resulted in dewatering of subducted plate of the ancient Asian Ocean. In the early Permian, Dongdashan area is under the background of active continental margin.
- bimodal magmatites,
- Northern margin of North China Craton,
- extension setting,
- active continental margin,
- the early Permian,
- geochemistry

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References(78)

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Early Permian Bimodal Magmatism in the Duolun Area of the Central Section of the Northern Margin of the North China Craton

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